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Libros sobre el tema "Soil respiration"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 25 de enero de 2025

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1

Naumov, A. V. Dykhanie pochvy: Sostavli︠a︡i︠u︡shchie, ėkologicheskie funkt︠s︡ii, geograficheskie zakonomernosti. Novosibirsk: Izd-vo Sibirskogo otd-nii︠a︡ Rossiĭskoĭ Akademii Nauk, 2009.

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2

Naumov, A. V. Dykhanie pochvy: Sostavli︠a︡i︠u︡shchie, ėkologicheskie funkt︠s︡ii, geograficheskie zakonomernosti. Novosibirsk: Izd-vo Sibirskogo otd-nii︠a︡ Rossiĭskoĭ Akademii Nauk, 2009.

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3

Rannelli, Dennis. Basal respiration and respiration response to added organic substrates as indicators of the health of smelter-affected soils, before and after revegetation. Sudbury, Ont: Laurentian University, Department of Biology, 1997.

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4

Zhou, Xuhui y Luo Yiqi. Soil Respiration and the Environment. Elsevier Science & Technology Books, 2010.

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5

Luo, Yiqi y Xuhui Zhou. Soil Respiration and the Environment. Academic Press, 2006.

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6

Soil Respiration and the Environment. Elsevier, 2006. http://dx.doi.org/10.1016/b978-0-12-088782-8.x5000-1.

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7

Soil Respiration and the Environment. Academic Press, 2006.

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8

Soil Respiration and the Environment. Emerald Publishing Limited, 2006.

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9

Forest Soil Respiration under Climate Changing. MDPI, 2018. http://dx.doi.org/10.3390/books978-3-03897-179-5.

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10

National Aeronautics and Space Administration (NASA) Staff. Boreas Te-5 Soil Respiration Data. Independently Published, 2018.

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11

Pascoe, Frank. Effects of forest soil compaction on gas diffusion, denitrification, nitrogen mineralization, and soil respiration. 1992.

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12

Boening, Dean W. Evaluation of an automated respiration method used in assessing the toxicity of zinc on soil microorganisms. 1992.

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13

Wood, Brian David. Carbon dioxide as a measure of microbial activity in the unsaturated zone. 1991.

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14

Dykhatelʹnyĭ gazoobmen i produktivnostʹ stepnykh fitot͡s︡enozov. Novosibirsk: "Nauka," Sibirskoe otd-nie, 1988.

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15

Kirchman, David L. Degradation of organic matter. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0007.

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The aerobic oxidation of organic material by microbes is the focus of this chapter. Microbes account for about 50% of primary production in the biosphere, but they probably account for more than 50% of organic material oxidization and respiration (oxygen use). The traditional role of microbes is to degrade organic material and to release plant nutrients such as phosphate and ammonium as well as carbon dioxide. Microbes are responsible for more than half of soil respiration, while size fractionation experiments show that bacteria are also responsible for about half of respiration in aquatic habitats. In soils, both fungi and bacteria are important, with relative abundances and activity varying with soil type. In contrast, fungi are not common in the oceans and lakes, where they are out-competed by bacteria with their small cell size. Dead organic material, detritus, used by microbes, comes from dead plants and waste products from herbivores. It and associated microbes can be eaten by many eukaryotic organisms, forming a detritus food web. These large organisms also break up detritus into small pieces, creating more surface area on which microbes can act. Microbes in turn need to use extracellular enzymes to hydrolyze large molecular weight compounds, which releases small compounds that can be transported into cells. Fungi and bacteria use a different mechanism, “oxidative decomposition,” to degrade lignin. Organic compounds that are otherwise easily degraded (“labile”) may resist decomposition if absorbed to surfaces or surrounded by refractory organic material. Addition of labile compounds can stimulate or “prime” the degradation of other organic material. Microbes also produce organic compounds, some eventually resisting degradation for thousands of years, and contributing substantially to soil organic material in terrestrial environments and dissolved organic material in aquatic ones. The relationship between community diversity and a biochemical process depends on the metabolic redundancy among members of the microbial community. This redundancy may provide “ecological insurance” and ensure the continuation of key biogeochemical processes when environmental conditions change.
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16

Wilsey, Brian J. Nutrient Cycling and Energy Flow in Grasslands. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198744511.003.0004.

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Net primary productivity (NPP) is the amount of C or biomass that accumulates over time and is photosynthesis—autotroph respiration. Annual NPP is estimated by summing positive biomass increments across time periods during the growing season, including offtake to herbivores, which can be high in grasslands. Remote sensing techniques that are used to assess NPP are discussed by the author. Belowground productivity can be high in grasslands, and it is important to carbon storage. Across grasslands on a geographic scale, NPP, N mineralization, and soil organic C all increase with annual precipitation. Within regions, NPP can be strongly affected by the proportion of C4 plant species and animal species composition and diversity. Humans are adding more N to the environment than all the natural forms of addition (fixation and lightning) combined. Animals, especially herbivores, can have strong effects on how plants respond to changes in changes in resource availability.
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